A glacier is a large, slow moving river of ice, formed from compacted layers of snow, that slowly deforms and flows in response to gravity. River of Ice
alpine glaciers: found in mountain terrains Two types of glaciers alpine glaciers: found in mountain terrains continental glaciers: cover larger areas
alpine glaciers: found in mountain terrains Two types of glaciers alpine glaciers: found in mountain terrains continental glaciers: cover larger areas
alpine glaciers: found in mountain terrains Two types of glaciers alpine glaciers: found in mountain terrains continental glaciers: cover larger areas
alpine glaciers: found in mountain terrains Two types of glaciers alpine glaciers: found in mountain terrains continental glaciers: cover larger areas
alpine glaciers: found in mountain terrains Two types of glaciers alpine glaciers: found in mountain terrains continental glaciers: cover larger areas
alpine glaciers: found in mountain terrains Two types of glaciers alpine glaciers: found in mountain terrains continental glaciers: cover larger areas
Changes in the Qori Kalis Glacier, Quelccaya Ice Cap, Peru, are shown between 1978 (top) and 2002. The glacier retreat during this time was 1,100 meters. Photo credit: Professor L. Thompson
Breidamerkurjökull Ice Cap and shows the changes over a three-year time period, between 1997 and 2000 .
River of Ice U-Shaped Valleys
Tongass National Forest, Alaska, USA.
River of Ice U-Shaped Valleys Scratched Rock
Glacial Scratches and Grooves
River of Ice U-Shaped Valleys Scratched Rock Unsorted Sediment
River of Ice U-Shaped Valleys Scratched Rock Unsorted Sediment Erratics
A glacial erratic is a piece of rock that deviates from the size and type of rock native to the area in which it rests; the name "erratic" is based on the errant location of these boulders. These rocks were carried to their current locations by glacial ice. Erratics can range in size from pebbles to large boulders.
River of Ice U-Shaped Valleys Scratched Rock Unsorted Sediment Erratics